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过去35年中国黑土区耕地开垦对土壤有机碳的影响

Effects of cropland reclamation on soil organic carbon in China's black soil region over the past 35 years.

作者信息

Wang Xiang, Li Sijia, Wang Liping, Zheng Miao, Wang Zongming, Song Kaishan

机构信息

Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, China.

University of Chinese Academy of Sciences, Beijing, China.

出版信息

Glob Chang Biol. 2023 Sep;29(18):5460-5477. doi: 10.1111/gcb.16833. Epub 2023 Jun 25.

Abstract

The long-term use of cropland and cropland reclamation from natural ecosystems led to soil degradation. This study investigated the effect of the long-term use of cropland and cropland reclamation from natural ecosystems on soil organic carbon (SOC) content and density over the past 35 years. Altogether, 2140 topsoil samples (0-20 cm) were collected across Northeast China. Landsat images were acquired from 1985 to 2020 through Google Earth Engine, and the reflectance of each soil sample was extracted from the Landsat image that its time was consistent with sampling. The hybrid model that included two individual SOC prediction models for two clustering regions was built for accurate estimation after k-means clustering. The probability hybrid model, a combination between the hybrid model and classification probabilities of pixels, was introduced to enhance the accuracy of SOC mapping. Cropland reclamation results were extracted from the land cover time-series dataset at a 5-year interval. Our study indicated that: (1) Long-term use of cropland led to a 3.07 g kg and 6.71 Mg C ha decrease in SOC content and density, respectively, and the decrease of SOC stock was 0.32 Pg over the past 35 years; (2) nearly 64% of cropland had a negative change in terms of SOC content from 1985 to 2020; (3) cropland reclamation track changed from high to low SOC content, and almost no cropland was reclaimed on the "Black soils" after 2005; (4) cropland reclamation from wetlands resulted in the highest decrease, and reclamation period of years 31-35 decreased when SOC density and SOC stock were 16.05 Mg C ha and 0.005 Pg, respectively, while reclamation period of years 26-30 from forest witnessed SOC density and stock decreases of 8.33 Mg C ha and 0.01 Pg, respectively. Our research results provide a reference for SOC change in the black soil region of Northeast China and can attract more attention to the area of the protection of "Black soils" and natural ecosystems.

摘要

长期使用农田以及从自然生态系统开垦农田导致了土壤退化。本研究调查了过去35年长期使用农田以及从自然生态系统开垦农田对土壤有机碳(SOC)含量和密度的影响。在中国东北共采集了2140个表层土壤样本(0 - 20厘米)。通过谷歌地球引擎获取了1985年至2020年的陆地卫星图像,并从时间与采样一致的陆地卫星图像中提取每个土壤样本的反射率。在进行k均值聚类后,构建了包含两个聚类区域的两个单独SOC预测模型的混合模型,用于准确估计。引入概率混合模型,即混合模型与像素分类概率的结合,以提高SOC制图的准确性。从土地覆盖时间序列数据集中每隔5年提取一次农田开垦结果。我们的研究表明:(1)长期使用农田导致SOC含量和密度分别下降3.07克/千克和6.71兆克碳/公顷,在过去35年中SOC储量减少了0.32拍克;(2)从1985年到2020年,近64%的农田SOC含量出现负变化;(3)农田开垦轨迹从高SOC含量变为低SOC含量,2005年后“黑土”上几乎没有开垦农田;(4)从湿地开垦农田导致的下降幅度最大,在31 - 35年的开垦期内,SOC密度和SOC储量分别为16.05兆克碳/公顷和0.005拍克,而从森林开垦26 - 30年期间,SOC密度和储量分别下降8.33兆克碳/公顷和0.01拍克。我们的研究结果为中国东北黑土区SOC变化提供了参考,能够吸引更多人关注“黑土”和自然生态系统保护区域。

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